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Determination and analysis of bearing capacity of calcarenites off the Florida Keys
J.S. Booth, R.A. Farrow, G.N. Wiley, R.C. Circe
1982, Open-File Report 82-309
A specially designed instrument was used to determine the in situ bearing capacity at 12 sites in the carbonate sand seaward of the Florida Keys. The resulting data set not only represents unique information in such an environment, but also provided an opportunity to determine whether bearing capacity is controlled...
Digital colored residual and regional Bouguer gravity maps of the conterminous United States: Comments on significant features
T.G. Hildenbrand, R.W. Simpson, R. H. Godson, M. F. Kane
1982, Open-File Report 82-284
The gravity maps were prepared from data obtained primarily from data files maintained by the Defense Mapping Agency of the Department of Defense and the Canadian Gravity Data Centre of the Earth Physics Branch of the Department of Energy, Mines, and Resources (Canada). The maps have been used in studies...
Potential geologic hazards and constraints for blocks in proposed North Atlantic OCS Oil and gas lease sale 52
G.B. Carpenter, A.P. Cardinell, D.K. Francois, L.K. Good, R.L. Lewis, N.T. Stiles
1982, Open-File Report 82-36
Analysis of high-resolution geophysical data collected over 540 blocks tentatively selected for leasing in proposed OCS Oil and Gas Lease Sale 52 (Georges Bank) revealed a number of potential geologic hazards to oil and gas exploration and development activities: evidence of mass movements and shallow gas deposits on the continental...
Assessment of the petroleum, coal, and geothermal resources of the Economic Community of West African States (ECOWAS) region
R. E. Mattick (compiler)
1982, Open-File Report 82-714
Approximately 85 percent of the land area of the ECOWAS (Economic Community of West African States) region is covered by basement rocks (igneous and highly metamorphosed rocks) or relatively thin layers of Paleozoic, Upper Precambrian, and 'Continental Intercalaire? sedimentary rocks. These areas have little or no petroleum potential. Areas of...
Depth and temperature of permafrost on the Alaskan Arctic Slope; preliminary results
Arthur H. Lachenbruch, J.H. Sass, L.A. Lawver, M.C. Brewer, T.H. Moses
1982, Open-File Report 82-1039
As permafrost is defined by its temperature, the only way to determine its depth is to monitor the return to equilibrium of temperatures in boreholes that penetrate permafrost. Such measurements are under way in 25 wells on the Alaskan Arctic Slope; 21 are in Naval Petroleum Reserve Alaska (NPRA), and...